Petrography: (A. Irving and S. Kuehner, UWS) Patchy, recrystallized texture with regions of different grain size, which do not appear to be separate clasts. No chondrules are present, but some of the finer grained regions may represent former chondrules. Constituent mineral are olivine, orthopyroxene, clinopyroxene, sodic plagioclase, chromite, altered kamacite, taenite and troilite.